Titlebook: Studies of Cave Sediments; Physical and Chemica Ira D. Sasowsky,John Mylroie Conference proceedings 2004 Springer Science+Business Media Ne

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Lithofacies and Transport of Clastic Sediments in Karstic Aquifers,ratified clays through boulders carried as a slurry during high energy flood events, (ii) thalweg facies: coarse gravel to cobble size material, well winnowed, forming armoring on underground streams that moves only during flood flow, (iii) channel facies: usually well sorted and often well stratifi

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Sediment and Sediment-Associated Contaminant Transport Through Karst,) has recently ruled that total maximum daily loads (TMDLs) are required even for stream segments impacted only by high suspended sediment concentrations. Furthermore, mobile sediment in karst may act as a vector for the transport of hydrophobic (“water fearing”) contaminants (Ford and Williams, 198

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Palaeomagnetic Analysis of Sediments in The Buchan Caves, Southeastern Australia, Provides a Prelatams, 1989; Atkinson et al, 1978; Gascoyne et al, 1981; Gascoyne, 1984). However, there is an accumulating body of evidence that much cave development in Australia occurred during the Tertiary (Webb et al, 1991) or even earlier (Osborne and Branagan, 1988; Osborne, 1990), well beyond the limits of ur

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Paleoclimate Records from Speleothems in Limestone Caves, and to a lesser extent Sr/Mg concentrations provide temperature information. Color banding resulting from variations in humic acid concentration and luminescence banding resulting from variations in fulvic acid concentration provide precipitation records with a resolution of one year or better. At

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